Magnesium isotope evidence that accretional vapour loss shapes planetary compositions

It has long been recognised that Earth and other differentiated planetary bodies are chemically fractionated compared to primitive, chondritic meteorites and by inference the primordial disk from which they formed. An important question has been whether the notable volatile depletions of planetary b...

Descripción completa

Detalles Bibliográficos
Autores principales: Hin, Remco C., Coath, Christopher D., Carter, Philip J., Nimmo, Francis, Lai, Yi-Jen, Pogge von Strandmann, Philip A.E., Willbold, Matthias, Leinhardt, Zoë M., Walter, Michael J., Elliott, Tim
Formato: Online Artículo Texto
Lenguaje:English
Publicado: 2017
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5624506/
https://www.ncbi.nlm.nih.gov/pubmed/28959965
http://dx.doi.org/10.1038/nature23899

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5624506/
https://www.ncbi.nlm.nih.gov/pubmed/28959965
http://dx.doi.org/10.1038/nature23899

Ejemplares similares